Isotope Features (Δ13С, Δ18О) of Continental Carbonates From Permian and Triassic Boundary Deposits Northeast of Russian Plate: Paleoclimatic and Biotic Causes, Chemostratigraphy

Литология и полезные ископаемые
doi 10.31857/s0024-497x20196568-591
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The Russian Academy of Sciences

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